Publication Date:
2023-09-23
Description:
Magnetic measurements of U-channel samples were measured by the Bartington MS2 magnetic susceptibility system with an ASC auto-tracking rail and a cryogenic magnetometer (2G 755 SRM) in the shielding room of the paleomagnetic laboratory at the Institute of Earth Sciences, Academia Sinica, Taiwan. The Anhysteretic Remanent Magnetization (ARM) was applied with a DC bias field of 1 Gauss under a 100 mT alternating field. All U-channel measurements are within 1 cm interval.
Keywords:
AGE; Anhysteretic remanent magnetization; Anhysteretic remanent magnetization/magnetic susceptibility ratio; Bartington MS2C sensor; Declination; DEPTH, sediment/rock; environmental magnetism; Giant piston corer; GPC; IMAGES VII - WEPAMA; Inclination; Magnetic susceptibility; marine sediments; Marion Dufresne (1995); MD012414; MD01-2414; MD122; Mid-Brunhes Transition; mid-Pleistocene transition; Okhotsk Sea; paleomagnetism; Relative paleointensity proxy; Sea ice; Sea of Ochotsk; Super-interglacial; terrigenous detritus
Type:
Dataset
Format:
text/tab-separated-values, 31659 data points
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